Persistent Slabs
- Hochgebirge
- Waldgrenze
- Unterhalb der Waldgrenze
- Wahrscheinlichkeit
- Possible
- Größe
- 2–3
The weak snow buried near the ground continues to be the primary avalanche concern in this zone. This layer has produced both human triggered and natural avalanches in this zone in the past few days:
- Saturday, a skier on Titus Ridge intentionally triggered a large avalanche. The slide initiated as a stiff wind slab that formed during last week's wind event and then "stepped down" to the December weak layer. Photos and more details are available here. I looked at the slide that afternoon—watch the video I made.
- Yesterday, Sun Valley Heli reported seeing a recent large, natural avalanche that failed near the Baker divide, likely involving this weak snow (photo here).
The depth of the snowpack is highly variable in this zone. This is important because the more deeply this weak snow is buried the more difficult it is to impact. Conversely, in areas where the snowpack is thinner, the weak layer is much more "accessible" to a skier or rider. Last week's prolonged wind event stripped many slopes (bringing the weak layer closer to the surface) and deposited hard slabs on many others (adding weight to the weak layer). Today's snowfall will mask the obvious signs of what happened during the wind event, which will make it more difficult to determine what happened on the slope that you are traveling on. This high degree of variability creates a snowpack who's behavior is difficult to predict. This fact has kept many experienced skiers and riders from entering into consequential avalanche terrain, despite the gradually decreasing danger.
So what sort of areas should you be most worried about right now? The two avalanches described above share a number of characteristics: they failed in steep (over 35 degrees), rocky, wind-affected terrain. This is exactly the type of terrain where you are most likely to encounter this problem today.
(2/13/2021) This avalanche was intentionally triggered by a skier stomping on the cornices/wind slab above. It failed on an E/NE facing slope at 9,700' above Titus Lake. The slide initiated in the stiff wind slabs that formed during last week's wind event and then stepped down to the weak snow near the ground as it traveled downslope.